西太平洋暖池海温对华南前汛期降水影响的数值试验
NUMERICAL STUDY OF INFLUENCE OF THE SSTA IN WESTERN PACIFIC WARM POOL ON PRECIPITATION IN THE FIRST FLOOD PERIOD IN SOUTH CHINA
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摘要: 简要地介绍了全球大气环流模式CCM3,由该模式模拟得到降水、位势高度场和风场,分析它的模拟性能。根据华南前汛期(4~6月)降水与西太平洋暖池敏感海区(西区)海温的负相关关系,设计了两组敏感性试验,讨论西区海温对华南前汛期降水影响的确定性和可能的物理机制。模拟结果表明,当西区为冷水年(暖水年)时,华南降水偏多(少),长江中下游相对偏少(多),相关最好的地区是广东省,与诊断分析结果相符。海温对降水的影响是通过大气环流场来实现的,因此,再用p-σ九层区域气候模式模拟了西区海温异常年大气环流对华南前汛期降水的影响,与CCM3模拟结果基本一致。Abstract: A brief introduction of a global atmospheric circulation model CCM3 is made and the CCM3 is used to simulate the precipitation of China, the height and the flow fields. The reliability of simulation is analyzed. According to the negative correlation between precipitation in the first flood period in South China (SC) and SSTA in a key region in western Pacific warm pool (West Region) , two sensitive experiments are designed to investigate the effects of the latter on the former and the possible physical mechanism is discussed. It is found that when the West Region is occupied with the negative SSTA, the rainfall in SC is far more than usual, while the rainfall in the middle and low reaches of the Yangtze River is relatively less. In warm water years, the case is reversed. The best correlative area of precipitation is located in Guangdong Province. It matches the diagnostic result well. The effect of SSTA on precipitation in SC is realized through the abnormality of atmosphere circulation and tested by ap-σ nine-layer regional climate model. Moreover, the simulative result of the p-σ model is basically coincident with that of the CCM3.
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[1] 梁建茵.南海海温变化及其对广东雨量的影响[J].热带气象,1991,7:246-253. [2] 谢炯光,纪忠萍.西北太平洋海温与广东省汛期降水的关系[J].热带气象学报,1999,15:56-63. [3] 丁纬钰,梁经萍.南海地区OLR变化与华南汛期降水的联系[J].热带气象学报,2002,18:276-282. [4] 邓立平,王谦谦.华南前汛期(4~6月)降水异常特征及其与我国近海海温的关系[J].热带气象学报,2002,18:47-55. [5] KIERHL JT,HACK J J,BONAN G B,et al.Description of the NCAR Community Climate Model(CCM3)[M].NCAR :NCAR Tech Note,1996.152. [6] 余建锐,董敏.CCM3大气环流模式月-季尺度预报初步试验[J].应用气象学报,2001,12:54-60. [7] 徐海明,何金海,董敏.印度半岛对亚洲夏季风进程影响的数值研究[J].热带气象学报,2001,17:117-124. [8] 徐海明,何金海,温敏,等.中南半岛影响南海夏季风建立和维持的数值研究[J].大气科学,2002,26:330-342. [9] 王晓悦.全球海温异常关键区的确定及其气候效应的模拟[D].南京:南京大学,2003.17-18. [10] 黄燕燕,钱永甫.长江流域、华北降水特征与南亚高压的关系分析[J].高原气象,2004,23:68-74. [11] 黄樱,钱永甫.南亚高压与华北夏季降水特征的关系[J].高原气象,2003,22:602-607. [12] 钱永甫.行星大气中地形效应的数值研究[M].北京:科学出版社,1988.49.
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